2018
DOI: 10.21513/2410-8758-2018-1-10-27
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Dynamic Processes in the Atmosphere Determining Summertime Precipitation Anomalies in the Western Siberia and Mongolia

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Cited by 7 publications
(2 citation statements)
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“…Beginning of this period refers to the mid-1990s of the 20th century [4,5]. It was found out that the low water in Baikal is due to long-term decrease in the amount of precipitation falling out in summer in the basin of the Selenga River [6][7][8][9]. As one of the main reasons for variations in rainfall in the Selenga basin, authors of [7][8][9] consider the activity of summer blockings in Eastern Siberia, in particular, and in the Eastern hemisphere in general.…”
Section: Discussionmentioning
confidence: 99%
“…Beginning of this period refers to the mid-1990s of the 20th century [4,5]. It was found out that the low water in Baikal is due to long-term decrease in the amount of precipitation falling out in summer in the basin of the Selenga River [6][7][8][9]. As one of the main reasons for variations in rainfall in the Selenga basin, authors of [7][8][9] consider the activity of summer blockings in Eastern Siberia, in particular, and in the Eastern hemisphere in general.…”
Section: Discussionmentioning
confidence: 99%
“…In both periods, typical structures of dipole blocking over Eastern Siberia and Mongolia correspond to ESM-blocks. Analysis of some ESM blocking events has shown that the cyclonic parts of ESM-blocks are characterized by advection of air masses from the East Asian monsoon region (EASM) [42]. Analysis that has been provided by Chen et al 2017 [43] indicated that there is a close relationship between the midlatitude summer cyclone activity over East Asia and the decadal variation of EASM; when the midlatitude summer cyclone activity over East Asia is strong (weak), EASM tends to be intensified (weakened).…”
Section: The Change Of European Blocking and Precipitation In The Rusmentioning
confidence: 99%